Inversion of seismic refraction and wide-angle reflection traveltimes for three-dimensional layered crustal structure
We present a method for the determination of crustal structure by simultaneous inversion of seismic refraction and wide-angle reflection traveltimes for 3-D interface geometry and layer velocity. Crustal structure is represented by layers in which velocity varies linearly with depth, separated by smooth interfaces with a cubic B-spline parametrization. Lateral variations in structure are therefore represented by variations in interface depth only. The model parametrization we have chosen means...[Show more]
|Collections||ANU Research Publications|
|Source:||Geophysical Journal International|
|01_Rawlinson_Inversion_of_seismic_2001.pdf||3.64 MB||Adobe PDF||Request a copy|
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